The Rustenburg Layered Suite formed as a stack of mush with transient magma chambers

The Rustenburg Layered Suite of the Bushveld Complex, South Africa, has long been regarded as a textbook result of fractional crystallization from a melt-dominated magma chamber. Here, the authors find that the Rustenburg Layered Suite can be derived from crustal assimilation by komatiitic magma to...

Descripción completa

Guardado en:
Detalles Bibliográficos
Autores principales: Zhuosen Yao, James E. Mungall, M. Christopher Jenkins
Formato: article
Lenguaje:EN
Publicado: Nature Portfolio 2021
Materias:
Q
Acceso en línea:https://doaj.org/article/795fb282f67c42dd8de815822fcd7d77
Etiquetas: Agregar Etiqueta
Sin Etiquetas, Sea el primero en etiquetar este registro!
id oai:doaj.org-article:795fb282f67c42dd8de815822fcd7d77
record_format dspace
spelling oai:doaj.org-article:795fb282f67c42dd8de815822fcd7d772021-12-02T14:09:00ZThe Rustenburg Layered Suite formed as a stack of mush with transient magma chambers10.1038/s41467-020-20778-w2041-1723https://doaj.org/article/795fb282f67c42dd8de815822fcd7d772021-01-01T00:00:00Zhttps://doi.org/10.1038/s41467-020-20778-whttps://doaj.org/toc/2041-1723The Rustenburg Layered Suite of the Bushveld Complex, South Africa, has long been regarded as a textbook result of fractional crystallization from a melt-dominated magma chamber. Here, the authors find that the Rustenburg Layered Suite can be derived from crustal assimilation by komatiitic magma to form magmatic mushes without requiring the existence of a magma chamber by using thermodynamic models.Zhuosen YaoJames E. MungallM. Christopher JenkinsNature PortfolioarticleScienceQENNature Communications, Vol 12, Iss 1, Pp 1-13 (2021)
institution DOAJ
collection DOAJ
language EN
topic Science
Q
spellingShingle Science
Q
Zhuosen Yao
James E. Mungall
M. Christopher Jenkins
The Rustenburg Layered Suite formed as a stack of mush with transient magma chambers
description The Rustenburg Layered Suite of the Bushveld Complex, South Africa, has long been regarded as a textbook result of fractional crystallization from a melt-dominated magma chamber. Here, the authors find that the Rustenburg Layered Suite can be derived from crustal assimilation by komatiitic magma to form magmatic mushes without requiring the existence of a magma chamber by using thermodynamic models.
format article
author Zhuosen Yao
James E. Mungall
M. Christopher Jenkins
author_facet Zhuosen Yao
James E. Mungall
M. Christopher Jenkins
author_sort Zhuosen Yao
title The Rustenburg Layered Suite formed as a stack of mush with transient magma chambers
title_short The Rustenburg Layered Suite formed as a stack of mush with transient magma chambers
title_full The Rustenburg Layered Suite formed as a stack of mush with transient magma chambers
title_fullStr The Rustenburg Layered Suite formed as a stack of mush with transient magma chambers
title_full_unstemmed The Rustenburg Layered Suite formed as a stack of mush with transient magma chambers
title_sort rustenburg layered suite formed as a stack of mush with transient magma chambers
publisher Nature Portfolio
publishDate 2021
url https://doaj.org/article/795fb282f67c42dd8de815822fcd7d77
work_keys_str_mv AT zhuosenyao therustenburglayeredsuiteformedasastackofmushwithtransientmagmachambers
AT jamesemungall therustenburglayeredsuiteformedasastackofmushwithtransientmagmachambers
AT mchristopherjenkins therustenburglayeredsuiteformedasastackofmushwithtransientmagmachambers
AT zhuosenyao rustenburglayeredsuiteformedasastackofmushwithtransientmagmachambers
AT jamesemungall rustenburglayeredsuiteformedasastackofmushwithtransientmagmachambers
AT mchristopherjenkins rustenburglayeredsuiteformedasastackofmushwithtransientmagmachambers
_version_ 1718391914620780544